Devolatilization of subducting slabs, Part I: Thermodynamic parameterization and open system effects
The amount of H2O and CO2 that is carried into deep mantle by subduction beyond subarc depths is of fundamental importance to the deep volatile cycle but remains debated. Given the large uncertainties surrounding the spatio‐temporal pattern of fluid flow and the equilibrium state within subducting s...
| Autors principals: | , , |
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| Format: | Journal article |
| Idioma: | English |
| Publicat: |
American Geophysical Union
2019
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